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Asteroid Models from the Lowell Photometric Database⋆ A&A 587, A48 (2016) Astronomy DOI: 10.1051/0004-6361/201527573 & c ESO 2016 Astrophysics Asteroid models from the Lowell photometric database J. Durechˇ 1, J. Hanuš2,3, D. Oszkiewicz4,andR.Vancoˇ 1 Astronomical Institute, Faculty of Mathematics and Physics, Charles University in Prague, V Holešovickáchˇ 2, 180 00 Prague 8, Czech Republic e-mail: [email protected] 2 Centre National d’Études Spatiales, 2 place Maurice Quentin, 75039 Paris Cedex 01, France 3 Laboratoire Lagrange, UMR 7293, Université de la Côte d’Azur, CNRS, Observatoire de la Côte d’Azur, Bd de l’Observatoire, CS 34229, 06304 Nice Cedex 04, France 4 Astronomical Observatory Institute, Faculty of Physics, A. Mickiewicz University, Słoneczna 36, 60-286 Poznan,´ Poland Received 16 October 2015 / Accepted 18 December 2015 ABSTRACT Context. Information about shapes and spin states of individual asteroids is important for the study of the whole asteroid population. For asteroids from the main belt, most of the shape models available now have been reconstructed from disk-integrated photometry by the lightcurve inversion method. Aims. We want to significantly enlarge the current sample (∼350) of available asteroid models. Methods. We use the lightcurve inversion method to derive new shape models and spin states of asteroids from the sparse-in-time photometry compiled in the Lowell Photometric Database. To speed up the time-consuming process of scanning the period parameter space through the use of convex shape models, we use the distributed computing project Asteroids@home, running on the Berkeley Open Infrastructure for Network Computing (BOINC) platform. This way, the period-search interval is divided into hundreds of smaller intervals. These intervals are scanned separately by different volunteers and then joined together. We also use an alternative, faster, approach when searching the best-fit period by using a model of triaxial ellipsoid. By this, we can independently confirm periods found with convex models and also find rotation periods for some of those asteroids for which the convex-model approach gives too many solutions. Results. From the analysis of Lowell photometric data of the first 100 000 numbered asteroids, we derived 328 new models. This almost doubles the number of available models. We tested the reliability of our results by comparing models that were derived from purely Lowell data with those based on dense lightcurves, and we found that the rate of false-positive solutions is very low. We also present updated plots of the distribution of spin obliquities and pole ecliptic longitudes that confirm previous findings about a non-uniform distribution of spin axes. However, the models reconstructed from noisy sparse data are heavily biased towards more elongated bodies with high lightcurve amplitudes. Conclusions. The Lowell Photometric Database is a rich and reliable source of information about the spin states of asteroids. We expect hundreds of other asteroid models for asteroids with numbers larger than 100 000 to be derivable from this data set. More models will be able to be reconstructed when Lowell data are merged with other photometry. Key words. minor planets, asteroids: general – methods: data analysis – techniques: photometric 1. Introduction shown that sparse photometry can be used to solve the lightcurve inversion problem and further simulations confirm this (Durechˇ Large all-sky surveys like Catalina, Pan-STARRS, etc. image et al. 2005, 2007). Afterwards, real sparse data were used either the sky every night to discover new asteroids and detect those alone or in combination with dense lightcurves and new asteroid that are potentially hazardous. The main output of these surveys models were derived (Durechˇ et al. 2009; Cellino et al. 2009; is a steadily increasing number of asteroids with known orbits. Hanuš et al. 2011, 2013c). The aim of these efforts was to de- Apart from astrometry that is used for orbit computation, these rive new unique models of asteroids, i.e., their sidereal rotation surveys also produce photometry of asteroids. This photome- periods, shapes, and direction of spin axis. try contains, in principle, information about asteroid rotation, shape, and surface properties. However, because of its poor qual- Another approach to utilize sparse data was to look for ity (when compared with a dedicated photometric measurements changes in the mean brightness as a function of the aspect angle, of a single asteroid) the signal corresponding to asteroid’s rota- which led to estimations of spin-axis longitudes for more than tion is usually drowned in noise and systematic errors. However, 350 000 asteroids (Bowell et al. 2014) from the so-called Lowell there have been recent attempts to use sparse-in-time photome- Observatory photometric database (Oszkiewicz et al. 2011). try to reconstruct the shape of asteroids. Kaasalainen (2004)has In this paper, we show that the Lowell photometric data set can also be used for solving the full inversion problem. By pro- Tables 1 and 2 are only available at the CDS via anonymous ftp to cessing Lowell photometry for the first 100 000 numbered as- cdsarc.u-strasbg.fr (130.79.128.5)orvia teroids, we derived new shapes and spin states for 328 aster- http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/587/A48 oids, which almost doubles the number of asteroids for which Czech National Team. the photometry-based physical model is known. Article published by EDP Sciences A48, page 1 of 6 A&A 587, A48 (2016) We describe the data, the inversion method, and the relia- 2.3. Asteroids@home bility tests in Sect. 2, the results in Sect. 3, and we conclude in Sect. 4. Asteroids@home is a volunteer-based computing project built on the Berkeley Open Infrastructure for Network Computing (BOINC) platform. Because the scanning of the period parameter space is the so-called embarrassingly parallel prob- 2. Method lem, we divided the whole interval of 2−100 h into smaller in- The lightcurve inversion method of Kaasalainen et al. (2001)that tervals (typically hundreds), which were searched individually we applied was reviewed by Kaasalainen et al. (2002)andmore on the computers of volunteers connected to the project. The units sent to volunteers had about the same CPU-time demand. recently by Durechˇ et al. (2016a). We used the same implemen- Results from volunteers were sent back to the BOINC server tation of the method as Hanuš et al. (2011), where the reader and validated. When all units belonging to one particular aster- is referred to for details. Here we describe only the general ap- oid were ready, they were connected and the global minimum proach and the details specific for our work. was found. The technical details of the project are described in Durechˇ et al. (2015) 2.1. Data As the data source, we used the Lowell Observatory photomet- 2.4. Ellipsoids ric database (Bowell et al. 2014). This is photometry provided To find the rotation period in sparse data, we also used an al- to Minor Planet Centre (MPC) by 11 of the largest surveys that ternative approach that was based on the triaxial ellipsoid shape were re-calibrated in the V-band using the accurate photometry model and a geometrical light-scattering model (Kaasalainen & of the Sloan Digital Sky Survey. Details about the data reduc- ˇ tion and calibration can be found in Oszkiewicz et al. (2011). Durech 2007). Its advantage is that it is much faster than using The data are available for about ∼330 000 asteroids. Typically, convex shapes because the brightness can be computed analyti- there are several hundreds of photometric points for each as- cally (it is proportional to the illuminated projected area, Ostro teroid. The length of the observing interval is ∼10–15 yr. The & Connelly 1984). On top of that, contrary to the convex mod- largest amount of data is for the low-numbered asteroids and de- elling, all shape models automatically fulfill the physical condi- tion of rotating along the principal axis with the largest momen- creases with increasing asteroid numbers. For example, the av- ffi erage number of data points is ∼480 for asteroids with number tum of inertia. The accuracy of this simplified model is su cient < ∼ > to reveal the correct rotation period as a significant minimum of 10 000 and 45 for those 300 000. The accuracy of the data χ2 is around 0.10−0.20 mag. in the period parameter space. That period is then used as a start point for the convex inversion for the final model. In many For each asteroid and epoch of observation, we computed cases when the convex models gives many equally good solu- the asteroid-centric vectors towards the Sun and the Earth in tions with different periods, this method provides a unique and the Cartesian ecliptic coordinate frame – these were needed to correct rotation period. compute the illumination and viewing geometry in the inversion code. 2.5. Restricted period interval 2.2. Convex models As mentioned above, the interval for period search was 2–100 h. However, for many asteroids, their rotation period is known To derive asteroid models from the optical data, we used the from observations of their lightcurves. The largest database of lightcurve inversion method of Kaasalainen & Torppa (2001) asteroid rotation periods is the Lightcurve Asteroid Database and Kaasalainen et al. (2001), the same way as Hanuš et al. (LCDB) compiled by Warner et al. (2009) and regularly up- (2011). Essentially, we searched for the best-fit model by dated2. If we take information about the rotation period as an densely scanning the rotation period parameter space. We de- a priori constraint, we can narrow the interval of possible peri- − cided to search in the interval of 2 100 h.
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